Analysis of Thermal Behaviour in the Active Layer of Degrading Mountain Permafrost

Mountain permafrost is highly susceptible to the effects of climate warming, because its thermal regime is close to 0 °C. This can be evidenced by the acceleration of average annual creep rates of several rock glaciers in the Swiss Alps, whereby some exhibit even more extreme signs of degradation. M...

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Bibliographic Details
Published in:Permafrost and Periglacial Processes
Main Authors: Xiaohai Zhou, Thomas Buchli, Wolfgang Kinzelbach, Fritz Stauffer, Sarah M. Springman
Format: Article in Journal/Newspaper
Language:unknown
Subjects:
Ice
Online Access:https://doi.org/10.1002/ppp.1827